Samples of red mud, by-products of alumina production from bauxite, are stu
died in the 120-1400 degrees C interval. An extensive characterization was
performed by thermal and X-ray diffraction analyses. The identification of
gaseous species released upon heating was carried out by coupling the therm
al analizer with a gas-chromatographic/mass spectrometer. Density evolution
was also determined as a function of the heat treatment. Results indicate
primary H2O release from aluminium hydroxides, followed by carbonate decomp
osition with CO2 evolution below 900 degrees C. Alkaline oxides, mainly CaO
and Na2O, lead to the formation of Ca3Al2O6 and NaAlSiO4 between 900 and 1
100 degrees C. At the highest temperatures, reduction of Fe3+ to Fe2+, invo
lving O-2 release, promotes the formation of Fe2TiO4, with the disappearanc
e of the rutile-TiO2 phase. The various solid state reactions, ascertained
at different stages of the heating process; and possible mass balances are
discussed with reference to the state diagrams of principal red mud compone
nts. (C) 2000 Elsevier Science Ltd. All rights reserved.